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Paleomagnetic studies on the syncollisional magmatic eruptions provide a direct way to understand when and where the Paleo‐Tethys closed. We report a well‐dated paleomagnetic pole from the southern Lancangjiang volcanic belt in western Yunnan of China. Stable Characteristic Remanent Magnetizations (ChRMs) were isolated from 21 sites at high temperatures following step‐wise thermal demagnetization. The data pass fold, reversal, and conglomerate tests and are interpreted to be primary thermal remanent magnetizations. The new paleomagnetic pole (46.1°N/176.2°E, K=44.9, A95=4.8°, N=21) yields a paleolatitude of 26.0 ± 4.8°N at the reference site (23.0°N/100.4°E) in the southern Lancangjiang area. This direct paleo‐latitudinal constraint on the Paleo‐Tethys suture zone in western Yunnan indicates that the north branch of the Paleo‐Tethys Ocean closed no later than the Carnian Age of Late Triassic, and confirms a geographic linkage between the North Qiangtang and Indochina Blocks at least during the Early Permian to Late Triassic. Plain Language Summary: The Asian continent is formed by the amalgamation of continental blocks such as the Tarim, North China, South China, Indochina, and Qiangtang. However, questions remained to answer: When did the ocean between them close? How did they drift from the south hemisphere to the north? In this study, we present a paleomagnetic constraint on the Paleo‐Tethys suture zone to quantify when and where the Paleo‐Tethys Ocean closed. The Paleo‐Tethys Ocean closed no later than the early Late Triassic at ~26°N. The Indochina and North Qiangtang drifted together from the south hemisphere to the north during the Permian‐Triassic. Key Points: The southern Lancangjiang volcanic belt formed at a paleolatitude of ~26ºN during the Carnian Stage of the Late TriassicThe north branch of the Paleo‐Tethys closed no later than the Carnian Stage of the Late TriassicA Permo‐Triassic geographic linkage between Indochina and N‐Qiangtang is confirmed [ABSTRACT FROM AUTHOR]